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Conceptualising Groundwater Flow Systems at a National (British Mainland) Scale
Conceptualising groundwater flow systems at a national (British mainland) scale Brighid Ó Dochartaigh and BGS Hydro-JULES team 11 September 2019 Seeking answers to 2 questions: How can an integrated & holistic approach to modelling terrestrial hydrology – including groundwater – improve: 1. Simulation of major flooding events, such as 2013-14 floods? 2. Assessment of water resources under drought conditions? Centre for Ecology & Hydrology | Hydro-JULES Conceptualising groundwater flow systems at a national (British mainland) scale 2 British mainland (WP4.1) 3D Parameterising Deep geological Saturated GW domain – Unsaturated framework Zone code technique Zone code model Conceptual FY18/19 models of groundwater (GW) flow Parameterising Model Sub-surface GW domain – instance code application FY19/20 Results Centre for Ecology & Hydrology | Hydro-JULES Conceptualising groundwater flow systems at a national (British mainland) scale 3 Britain’s diverse geology and hydrogeology Centre for Ecology & Hydrology | Hydro-JULES Conceptualising groundwater flow systems at a national (British mainland) scale 4 3D Geological Framework Model +1.5 km to -15 km 1:625,000 scale mapping Newell 2019 Centre for Ecology & Hydrology | Hydro-JULES Conceptualising groundwater flow systems at a national (British mainland) scale 5 Model includes 3D information from: borehole geology & geophysics; pre-existing cross sections; geological history & structure; seismic data Centre for Ecology & Hydrology | Hydro-JULES Conceptualising groundwater flow systems at a national (British mainland) scale 6 Geology: a physical framework for groundwater flow Centre for Ecology & Hydrology | Hydro-JULES Conceptualising groundwater flow systems at a national (British mainland) scale 7 Key groundwater conceptual model parameters Geology Geography Surface water Groundwater Aquifer Chemistry Flow Aquifer Topographic relief Recharge quantity, Groundwater flow Aquifer properties: e.g. -
RWM Eastern England Subregion 1
Eastern England SUBREGION 1 RWM | Eastern England Subregion 1 Contents 1 Eastern England Subregion 1 Introduction 2 Rock type 3 Rock structure Groundwater 4 Resources Natural processes 5 - 12 Figures 13 Glossary Clicking on words in green, such as sedimentary or lava will take the reader to a brief non-technical explanation of that word in the Glossary section. By clicking on the highlighted word in the Glossary, the reader will be taken back to the page they were on. Clicking on words in blue, such as Higher Strength Rock or groundwater will take the reader to a brief talking head video or animation providing a non-technical explanation. For the purposes of this work the BGS only used data which was publicly available at the end of February 2016. The one exception to this was the extent of Oil and Gas Authority licensing which was updated to include data to the end of June 2018. 1 RWM | Eastern England Subregion 1 Our work shows that we may find a suitable geological setting for a GDF in most of this subregion. Rock can be seen at the surface in some of this subregion such as the sea cliffs, cliffs in the North York Moors and in man-made excavations such as quarries or road cuttings. Combined with numerous deep boreholes and some geophysical investigations, this gives us an understanding of the rocks present and their distribution. There are clay-rich rock layers under most of the subregion in which we may be able to site a GDF. There are also layers of rock salt under most of the eastern coastal half of the subregion and extending off the coast, in which we may be able to site a GDF. -
Mineral Resources Report for Wiltshire
Mineral Resource Information in Support of National, Regional and Local Planning Wiltshire (comprising Wiltshire and the Borough of Swindon) Commissioned Report CR/04/049N BRITISH GEOLOGICAL SURVEY COMMISSIONED REPORT CR/04/049N Mineral Resource Information in Support of National, Regional and Local Planning Wiltshire (comprising Wiltshire and the Borough of Swindon) G E Norton, D G Cameron, A J Bloodworth, D J Evans, G K Lott, I J Wilkinson, H F Burke, N A Spencer, and D E Highley This report accompanies the 1;100 000 scale map: Wiltshire (comprising Wiltshire and the Borough of Swindon) Mineral Resources Key words Mineral resource planning, Wiltshire, Swindon. Front cover Westbury Cement Works, Lafarge Cement UK (Blue Circle Cements), and Westbury White Horse. Bibliographical reference G E NORTON, D G CAMERON, A J BLOODWORTH, D J EVANS, G K LOTT, I J WILKINSON, H F BURKE, N A SPENCER, and D E HIGHLEY. 2004. Mineral Resource Information in Support of National, Regional and Local Planning. Wiltshire (comprising Wiltshire and the Borough of Swindon) British Geological Survey Commissioned Report, CR/04/049N. 12pp. Keyworth, Nottingham British Geological Survey 2004 BRITISH GEOLOGICAL SURVEY The full range of Survey publications is available from the British Geological Survey offices BGS Sales Desks at Nottingham, Edinburgh and London; see contact details below or shop online at Keyworth, Nottingham NG12 5GG www.geologyshop.com 0115B936 3100......................... Fax 0115B936 3200 e-mail: sales @bgs.ac.uk The London Information Office also maintains a reference www.bgs.ac.uk collection of BGS publications including maps for Online shop: www.geologyshop.com consultation. -
Baseline Report Series: 14
Baseline Report Series: 14. The Corallian of Oxfordshire and Wiltshire Groundwater Systems and Water Quality Commissioned Report CR/04/262N Science Group: Air, Land & Water Technical Report NC/99/74/14 The Natural Quality of Groundwater in England and Wales A joint programme of research by the British Geological Survey and the Environment Agency BRITISH GEOLOGICAL SURVEY Commissioned Report CR/04/262N ENVIRONMENT AGENCY Science Group: Air, Land & Water Technical Report NC/99/74/14 This report is the result of a study jointly funded by the British Baseline Report Series: Geological Survey’s National Groundwater Survey and the 14. The Corallian of Oxfordshire and Environment Agency Science Group. No part of this work may be Wiltshire reproduced or transmitted in any form or by any means, or stored in a retrieval system of any nature, without the prior permission of the copyright proprietors. J Cobbing, M Moreau, P Shand, A Lancaster All rights are reserved by the copyright proprietors. Contributors Disclaimer The officers, servants or agents of both the British Geological Survey and the R Hargreaves (GIS) Environment Agency accept no liability whatsoever for loss or damage arising from the interpretation or use of the information, or reliance on the views contained herein. Environment Agency Dissemination status Internal: Release to Regions External: Public Domain ISBN: 978-1-84432-639-6 Product code: SCHO0207BLYL-E-P ©Environment Agency, 2004 Statement of use This document forms one of a series of reports describing the baseline chemistry of selected reference aquifers in England and Wales. Cover illustration Shelly, oolitic Corallian limestone near Baulking, Vale of White Horse. -
STRATEGIC STONE STUDY a Building Stone Atlas of NORTH-EAST YORKSHIRE
STRATEGIC STONE STUDY A Building Stone Atlas of NORTH-EAST YORKSHIRE Published May 2012 Derived from BGS digital geological mapping at 1:625,000 scale, British Geological Survey © NE Yorkshire Bedrock Geology NERC. All rights reserved Click on this link to visit NE Yorkshire’s geology and their contribution to known building stones, stone structures and building stone quarries (Opens in new window http://maps.bgs.ac.uk/buildingstone?County=North-EastYorkshire ) NE Yorkshire Strategic Stone Study 1 Stratigraphical column of the Permian (in part),Triassic, Jurassic and Cretaceous rocks and Quaternary deposits in North-east Yorkshire showing the common buildings stones (bold) and alternative stone names. The oldest rocks are at the bottom of the table. Gp., Group; Fm., Formation; Mbr., Member. North East Yorkshire: Permian, Triassic, Jurassic, Cretaceous & Quaternary Building Stones PERIOD GROUP FORMATION MEMBER Common/alternative Stone Name Calcareous Tufa; Aquarium Stone Till (Boulder Clay) and Fluvio-glacial sand Quaternary and gravel; boulders Tertiary Cleveland Dyke Whinstone Flamborough Chalk Fm. Flamborough Chalk; White Chalk Burnham Chalk Fm. Burnham Chalk; White chalk Chalk Group Welton ChalkFm. Cretaceous Ferriby Chalk Fm. Grey chalk ungrouped Hunstanton Fm. Speeton Clay Kimmeridge Clay ungrouped Ampthill Clay North Grimston Upper Calcareous Grit Upper Calcareous Grit Cementstone North Grimston Cementstone Formation Coral Rag Member Coral Rag Malton Oolite Member Malton Oolite; Hildenley Limestone; Corallian Hildenley Stone Group Middle Calcareous Grit Middle Calcareous Grit Coralline Oolite Formation Member Birdsall Calcareous Grit Birdsall Calcareous Grit Member Hambleton Oolite Hambleton Oolite Member Yedmandale Member Passage Beds; Wallstone Lower Calcareous Grit Fm. Lower Calcareous Grit Oxford Clay Fm. -
Stratigraphical Framework for the Middle Jurassic Strata of Great
Stratigraphical framework for the Middle Jurassic strata of Great Britain and the adjoining continental shelf Geology and Landscape Programme Research Report RR/11/06 BRITISH GEOLOGICAL SURVEY RESEARCH REPORT RR/11/06 The National Grid and other Stratigraphical framework for the Ordnance Survey data © Crown copyright and database rights 2012. Ordnance Survey Licence Middle Jurassic strata of Great No. 100021290 Britain and the adjoining Key words Geology, stratigraphy, lithostratigraphy, Inferior Oolite continental shelf Group, Great Oolite Group, Ravenscar Group, Great Estuarine Group, Sutherland Group, Ancholme Group, Jurassic. A J M Barron, G K Lott, J B Riding Front cover Hilltop Quarry, Leckhampton Hill, Cheltenham, Glos.: the Birdlip Limestone Formation overlain by the Aston Limestone Formation. (P775213, A J M Barron) Bibliographical reference BARRON, A J M, LOTT, G K, AND RIDING, J B. 2012. Stratigraphical framework for the Middle Jurassic strata of Great Britain and the adjoining continental shelf. British Geological Survey Research Report, RR/11/06. 187pp. ISBN 978 0 85272 695 2 Copyright in materials derived from the British Geological Survey’s work is owned by the Natural Environment Research Council (NERC) and/or the authority that commissioned the work. You may not copy or adapt this publication without first obtaining permission. Contact the BGS Intellectual Property Rights Section, British Geological Survey, Keyworth, e-mail [email protected]. You may quote extracts of a reasonable length without prior permission, provided -
Mineral Safeguarding Areas for North York Moors National Park Authority
Mineral Safeguarding Areas for North York Moors National Park Authority Minerals and Waste Programme Commissioned Report CR/13/073 BRITISH GEOLOGICAL SURVEY MINERALS AND WASTE PROGRAMME COMMISSIONED REPORT CR/13/073 Mineral Safeguarding Areas for North York Moors National Park Authority C E Wrighton, T P Bide, S Parry and K A Linley Contributor/editor The National Grid and other Ordnance Survey data © Crown R A Shaw and J M Mankelow Copyright and database rights 2013. Ordnance Survey Licence No. 100021290. Keywords Mineral resources; mineral safeguarding. Bibliographical reference WRIGHTON, C E, BIDE, T P, PARRY, S, AND LINLEY, K A. 2013. Mineral Safeguarding Areas for North York Moors National Park Authority . British Geological Survey Commissioned Report, CR/13/073. 51pp. Copyright in materials derived from the British Geological Survey’s work is owned by the Natural Environment Research Council (NERC) and/or the authority that commissioned the work. You may not copy or adapt this publication without first obtaining permission. Contact the BGS Intellectual Property Rights Section, British Geological Survey, Keyworth, e-mail [email protected]. You may quote extracts of a reasonable length without prior permission, provided a full acknowledgement is given of the source of the extract. Maps and diagrams in this book use topography based on Ordnance Survey mapping. © NYMNPA 2013. All rights reserved Keyworth, Nottingham British Geological Survey 2013 BRITISH GEOLOGICAL SURVEY The full range of our publications is available from BGS shops at British Geological Survey offices Nottingham, Edinburgh, London and Cardiff (Welsh publications only) see contact details below or shop online at www.geologyshop.com BGS Central Enquiries Desk Tel 0115 936 3143 Fax 0115 936 3276 The London Information Office also maintains a reference collection of BGS publications, including maps, for consultation. -
'TROPICAL YORKSHIRE' Fieldtrip to the Corallian Group (Upper Jurassic)
‘TROPICAL YORKSHIRE’ Fieldtrip to the Corallian Group (Upper Jurassic) of the North Yorkshire Moors Part of the 58th Annual Meeting of the Palaeontological Association, held at the University of Leeds 19th December 2014 J.D. Witts 20/11/14 TROPICAL YORKSHIRE – FIELDTRIP TO THE CORALLIAN GROUP (UPPER JURASSIC) OF THE NORTH YORKSHIRE MOORS INTRODUCTION Welcome to this one-day fieldtrip, run as part of the 58th Annual Meeting of the Palaeontological Association at the University of Leeds. Today we will visit three inactive quarries in the southern part of the North York Moors, to the East of Leeds, to look at various facies of the Oxfordian (Upper Jurassic) Corallian sediments in the area. We will start at Betton Farm Quarry, an SSSI site that has recently been cleared. Here there are metre-scale reef structures formed by the coral genera Isastraea and Thamnasteria, together with very fossiliferous inter-reef facies containing molluscs, echinoids and other fauna. Also in the quarry are examples of the surrounding oolitic facies of the Malton Oolite Member (Coralline Oolite Formation). After lunch at the quarry we will move to Ravenswick Quarry to look at tall quarry faces displaying weathered surfaces of the Malton Oolite, some beds of which are packed with large gastropods, and the overlying Coral Rag Member, which contains in-situ Rhabdophyllia phillipsi corals and the characteristic echinoid spines of Paracidaris florigemma. We will then drive a short way to Spaunton Quarry to look again at the Coral Rag, which here contains patch reefs and various inter-reef facies, and is overlain by the sandy sediments of the Newbridge and Spaunton Sandstone Members of the Upper Calcareous Grit Formation, from which ammonites can sometimes be collected. -
The Stratigraphy of the Kimmeridge Clay Formation (Jurassic) at Westbury, Wiltshire, U.K
Proceedings of the Geologists’ Association 127 (2016) 280–287 Contents lists available at ScienceDirect Proceedings of the Geologists’ Association jo urnal homepage: www.elsevier.com/locate/pgeola The stratigraphy of the Kimmeridge Clay Formation (Jurassic) at Westbury, Wiltshire, U.K. Ramues Gallois Gallois Geological Consultancy, 92 Stoke Valley Rd., Exeter EX4 5ER, United Kingdom A R T I C L E I N F O A B S T R A C T Article history: The former Blue Circle Cement quarry at Westbury, Wiltshire exposed extensive sections in the lower Received 14 September 2015 part of the Kimmeridge Clay Formation, and a continuously cored borehole proved the lowest part of the Received in revised form 22 December 2015 formation and the underlying succession down to the top of the Oxford Clay Formation. The succession Accepted 22 December 2015 exposed in the quarry between 1979 and 2001 ranged from the Cymodoce to Eudoxus zones, and that in Available online 18 March 2016 the borehole from the Baylei to Mutabilis zones. Taken together, the quarry and borehole proved the most complete section through the Kimmeridge Clay in a region where much of the formation has never Keywords: been exposed. The lithological and palaeontological successions proved at Westbury are closely similar Jurassic to those proved in continuously cored boreholes throughout the English outcrop and subcrop of the Kimmeridge Clay Formation Kimmeridgian formation and can be matched in detail with that exposed in the type area on the Dorset coast. When the Westbury quarry was in work the sections yielded a profuse ammonite fauna that enabled the Cymodoce– Stratigraphy Mutabilis and Mutabilis–Eudoxus zonal boundaries to be studied in detail. -
1 Diamicton from the Vale of Pickering and Tabular Hills, North
Diamicton from the Vale of Pickering and Tabular Hills, north-east Yorkshire: evidence for a Middle Pleistocene (MIS8) glaciation? John H. Powell, Jonathan R. Ford and James B. Riding 1British Geological Survey, Keyworth, Nottingham, NG12 5GG, United Kingdom *Corresponding author: e-mail: [email protected] (J.H. Powell) ABSTRACT Diamicton deposits (up to 6.90 m thick) in the Vale of Pickering and the Tabular Hills (North York Moors) have been confirmed by cored boreholes. The diamicton is interpreted as glacial till with a matrix consisting predominantly of grey-brown, yellow-brown and dark grey, stiff to very stiff clay and sandy clay with occasional thin beds of laminated sand and clay. Sub-rounded to sub-angular erratic clasts were sourced predominantly from local Upper Jurassic Corallian Group bedrock exposed in the southern part of the North York Moors. Clasts include well-rounded, pebbles of Jurassic sandstone, mudstone and sparse Jurassic coal derived from outcrops on the North York Moors. Fragments of underlying Upper Jurassic mudstone bedrock form the predominant clasts in the lower part of the till. The paucity of exotic clasts and a local derivation suggests a relatively small glacier - perhaps a temperate-plateau ice-field, was established on the Tabular Hills. The glacier subsequently advanced southwards to the Vale of Pickering depositing locally derived subglacial traction till at the base, passing up to lodgement till. Local preservation of the degraded till outcrops in the Vale of Pickering, the overconsolidated nature of the clay till matrix, striated pebbles and the presence of sub-rounded pebbles suggests deposition during a glacial cold stage post-MIS 12 (Anglian) and pre-MIS 2 (Devensian). -
A Stratigraphical Framework for the Lower Cretaceous of England
A stratigraphical framework for the Lower Cretaceous of England Research Report RR/08/03 HOW TO NAVIGATE THIS DOCUMENT Bookmarks The main elements of the table of contents are book- marked enabling direct links to be followed to the principal section headings and sub- headings, figures, plates and tables irrespective of which part of the document the user is viewing. In addition, the report contains links: from the principal section and subsection headings back to the contents page, from each reference to a figure, plate or table directly to the corresponding figure, plate or table, from each figure, plate or table caption to the first place that figure, plate or table is mentioned in the text and from each page number back to the contents page. RETURN TO CONTENTS PAGE BRITISH GEOLOGICAL SURVEY RESEARCH REPORT RR/08/03 The National Grid and other Ordnance Survey data are used with the permission of the Controller of Her Majesty’s Stationery Office. Licence No: 100017897/2008. Keywords A stratigraphical framework for the United Kingdom, England, Yorkshire, Lincolnshire, East Anglia, Southern England. Lower Cretaceous of England Geology, Stratigraphy, Lower Cretaceous, Early Cretaceous. P M Hopson, I P Wilkinson and M A Woods Front cover Ferruginous Sand Formation exposed above a significant landslide founded in the Atherfield Clay Formation, Red Cliff, Sandown Bay, Isle of Wight (P683788). Bibliographical reference HOPSON , P M, WILKINSON , I P, and WOODS , M A. 2008. A stratigraphical framework for the Lower Cretaceous of England. British Geological Survey. British Geological Survey Research Report, RR/08/03. ISBN 0 85272 623 5 Copyright in materials derived from the British Geological Survey’s work is owned by the Natural Environment Research Council (NERC) and/or the authority that commissioned the work. -
A Building Stone Atlas of Oxfordshire
Strategic Stone Study A Building Stone Atlas of Oxfordshire First published by English Heritage March 2011 Rebranded by Historic England December 2017 Introduction The oldest rocks in Oxfordshire crop out in the north of the county and are of Lower Jurassic age, around 200 million years old. Younger Jurassic and Cretaceous formations progressively crop out towards the south. The harder limestone and chalk lithologies form escarpments, whilst clay underlies the intervening vales. The character of Oxfordshire’s stone buildings is very much determined by the nature of the local stone, which leads to a fascinating variation of styles across the county. With the exception of the Jurassic ooidal freestone quarried around Taynton, few building stones were of sufficient quality to be used much beyond their immediate source area. Now only a handful of building stone quarries are still active in the county, supplying Marlstone and the Chipping Norton Limestone. Unfortunately the other building stones described in the following pages are no longer available from working local quarries. The following summary of the principal local building stones is based largely on Arkell’s work, Oxford Stone and The Geology of Oxford, and Powell’s recent Geology of Oxfordshire. The oldest stones are described first, progressing towards the stratigraphically youngest to the south. XXX Strategic Stone Study 1 Oxfordshire Bedrock Geology Map Derived from BGS digital geological mapping at 1:625,000 scale, British Geological Survey ©NERC. All rights reserved Oxfordshire Strategic Stone Study 2 Lower Jurassic The distinctive warm-coloured Marlstone characterises the cottages in many villages such as Great Tew, Deddington, Lias Group Adderbury, Bloxham, Wroxton, Hook Norton and Hornton, as well as churches such as St.